Developments in the Cretaceous Stratigraphy of Crimea. Part 2. Upper Cretaceous and Conclusions

被引:0
作者
Baraboshkin, E. Yu. [1 ,3 ]
Guzhikov, A. Yu. [2 ]
Ryabov, I. P. [2 ]
Tesakova, E. M. [1 ,3 ]
Vishnevskaya, V. S. [3 ]
Ustinova, M. A. [3 ]
机构
[1] Moscow MV Lomonosov State Univ, Geol Fa?, Moscow 119234, Russia
[2] Saratov NG Chernyshevskii State Univ, Geol Fa?, Saratov 410012, Russia
[3] Russian Acad Sci, Geol Inst, Moscow 119017, Russia
基金
俄罗斯科学基金会;
关键词
biostratigraphy; ammonites; belemnites; ostracods; foraminifers; gilianelles; nannoplankton; magnetostratigraphy; SANTONIAN-CAMPANIAN BOUNDARY; ALAN-KYR SECTION; OCEANIC ANOXIC EVENT; INFRAZONAL BIOSTRATIGRAPHY; BENTHIC FORAMINIFERS; RIVER SECTION; 1ST RECORD; CONIACIAN; RADIOLARIANS; DEPOSITS;
D O I
10.1134/S0869593824700217
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
This is the second part of the paper on the Cretaceous of the Mountainous Crimea. A lot of new data has been received during last ten years. This paper summarizes the state of knowledge of the Upper Cretaceous stratigraphy, selected biostratigraphic groups (ammonites, belemnites, ostracods, foraminifers, gilianelles, nannoplankton) and magnetostratigraphy. Ammonite and belemnite biostratigraphic subdivisions are proposed for the first time for the Crimean Upper Cretaceous. Foraminifera-based biostratigraphy is updated, and new biostratigraphic units are proposed and correlated with the European scale. Stratigraphic hiatuses are recognised in the succession of southwestern Crimea: the base and the top of lower Cenomanian, upper Coniacian-lower Santonian, Campanian/Maastrichtian and Cretaceous/Paleogene boundary intervals.
引用
收藏
页码:733 / 777
页数:45
相关论文
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